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Understanding post-mining landforms: Utilising pre-mine geomorphology to improve rehabilitation outcomes (3) · Implementation and performance of adaptive mesh refinement in the Ice Sheet System Model (ISSM v4.14) (3) · Simulating tidal and storm surge hydraulics with a simple 2D inertia based model, in the Humber Estuary, U.K (3) · A Coupled Atmosphere–Wave–Ocean Modeling System: Simulation of the Intensity of an Idealized Tropical Cyclone (3) · Modelling headwater channel response and suspended sediment yield to in-channel large wood using the Caesar-Lisflood landscape evolution model (3) · Impacts of Seagrass Dynamics on the Coupled Long‐Term Evolution of Barrier‐Marsh‐Bay Systems (3) · Modeling sediment movement and channel response to rainfall variability after a major earthquake (3) · Assessing climate change impacts on the stability of small tidal inlets: Part 2 - Data rich environments (3) · Assessing the potential long-term effects of sea-level rise on salt marsh’s coastal protective capacity under different climate pathway scenarios (3) · Catchment reconstruction — erosional stability at millennial time scales using landscape evolution models (3) · Bayeslands: A Bayesian inference approach for parameter uncertainty quantification in Badlands (3) · Integrating the SLIDE model within CAESAR-Lisflood: Modeling the ‘rainfall-landslide-flash flood’ disaster chain mechanism under landscape evolution in a mountainous area (3) · Rainfall spatial-heterogeneity accelerates landscape evolution processes (3) · Modelling the impact of seismic triggered landslide location on basin sediment yield, dynamics and connectivity (3) · Wave Energy Assessment around the Aegadian Islands (Sicily) (3) · The Downscaling Study for Typhoon-Induced Coastal Inundation (3) · SedFoam: A multi-dimensional Eulerian two-phase model for sediment transport and its application to momentary bed failure (3) · Three-dimensional scour simulations with a two-phase flow model (3) · How to account for particle size effects in a landscape evolution model when there is a wide range of particle sizes (3)
 
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